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dc.contributor.authorPeszynska, Malgorzata
dc.contributor.authorHong, Wei-Li
dc.contributor.authorTorres, Marta E.
dc.contributor.authorKim, Ji-Hoon
dc.date.accessioned2022-05-05T09:10:22Z
dc.date.available2022-05-05T09:10:22Z
dc.date.issued2016-06-13
dc.description.abstractIn this paper, we present a reduced model of methane hydrate formation in variable salinity conditions, with details on the equilibrium phase behavior adapted to a case study from Ulleung Basin. The model simplifies the comprehensive model considered by Liu and Flemings using common assumptions on hydrostatic pressure, geothermal gradient, and phase incompressibility, as well as a simplified phase equilibria model. The two-phase threecomponent model is very robust and efficient as well as amenable to various numerical analyses, yet is capable of simulating realistic cases. We compare various thermodynamic models for equilibria as well as attempt a quantitative explanation for anomalous spikes of salinity observed in Ulleung Basin.en_US
dc.identifier.citationPeszynska M, Hong H, Torres ME, Kim. Methane hydrate formation in Ulleung basin under conditions of variable salinity: reduced model and experiments. Transport in Porous Media. 2016;114(1):1-27en_US
dc.identifier.cristinIDFRIDAID 1368197
dc.identifier.doi10.1007/s11242-016-0706-y
dc.identifier.issn0169-3913
dc.identifier.issn1573-1634
dc.identifier.urihttps://hdl.handle.net/10037/25018
dc.language.isoengen_US
dc.publisherSpringeren_US
dc.relation.journalTransport in Porous Media
dc.rights.accessRightsopenAccessen_US
dc.rights.holderCopyright 2016 The Author(s)en_US
dc.titleMethane hydrate formation in Ulleung basin under conditions of variable salinity: reduced model and experimentsen_US
dc.type.versionpublishedVersionen_US
dc.typeJournal articleen_US
dc.typeTidsskriftartikkelen_US
dc.typePeer revieweden_US


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